5. Macpherson, J.—"Tremblements de terre en Espagne." Paris, Acad. Sci., Compt. Rend., vol. c., 1885, pp. 397-399.
6. Nogués, A.F.—"Phénomènes géologiques produits par les tremblements de terre de l'Andalousie, du 25 décembre 1884 au 16 janvier 1885." Ibid., pp. 253-256.
7. Rossi, M.S. de.—"Gli odierni terremoti di Spagna ed il loro eco in Italia." Bull. Vulc. Ital., anno xii., 1885, pp. 17-31.
8. Taramelli, T., and G. Mercalli.—"I terremoti Andalusi cominciati il 25 dicembre 1884." Roma, R. Accad. Lincei, Mem., vol: iii., 1885, pp. 116-222.
9. Paris, Acad. Sci., Compt. Rend., vol. c., 1885, pp. 24-27, 136-138, 196-197, 256-257, 598-601, 1113-1120, 1436 (the last three by F. Fouqué).
FOOTNOTES:
[31] These times correspond to about 9.10 and 9.25 P.M., Greenwich mean time. The earthquake stopped a clock at the Royal Observatory of San Fernando (Cadiz), at 8h. 43m. 54.5s. mean local time, corresponding to 9h. 8m. 44s., G.M.T.
[32] The earthquake is also said to have been registered at the observatory of Moncalieri, near Turin, but I have not been able to ascertain the time of occurrence. A movement felt at about 10.20 P.M. at Ramsbury, in Wiltshire, was attributed to the earthquake, though the time is about an hour too late. On December 26th, an astronomical clock was stopped at Brussels and its pillar displaced; and, on the evening of the same day, the large telescope at the observatory was also found to have been shifted. These effects, it is suggested, were caused by the Andalusian earthquake, but the connection between them seems to me very doubtful.
[33] The French observers have also applied a method depending on the time of occurrence of the shock. Joining places where the recorded times were the same, they notice that the perpendicular bisectors of these lines intersect within an area which agrees practically with that determined by the azimuths. The inaccuracy of the time-records must, however, lessen the significance of this result.